October 2018 Journal of the Institution of Environmental Sciences CONTENTS > How and Why Are the Oceans Changing?
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Geology, Geochemistry and Earthquake History of Loieihi Seamount, Hawaiei's Youngest Volcano
ARTICLE IN PRESS Chemie der Erde ] (]]]]) ]]]–]]] www.elsevier.de/chemer INVITED REVIEW Geology, geochemistry and earthquake history of Lo¯"ihi Seamount, Hawai"i’s youngest volcano Michael O. Garciaa,Ã, Jackie Caplan-Auerbachb, Eric H. De Carloc, M.D. Kurzd, N. Beckera aDepartment of Geology and Geophysics, University of Hawai"i, Honolulu, HI 96822, USA bAlaska Volcano Observatory, U.S.G.S., Alaska Science Center, Anchorage, AK 99508, USA cDepartment of Oceanography, University of Hawai"i, Honolulu, HI 96822, USA dDepartment of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA Received 6 June 2005; accepted 20 September 2005 Abstract A half-century of investigations are summarized here on the youngest Hawaiian volcano, Lo¯"ihi Seamount. It was discovered in 1952 following an earthquake swarm. Surveying in 1954 determined it has an elongate shape, which is the meaning of its Hawaiian name. Lo¯"ihi was mostly forgotten until two earthquake swarms in the 1970s led to a dredging expedition in 1978, which recovered young lavas. The recovery of young lavas motivated numerous expeditions to investigate the geology, geophysics, and geochemistry of this active volcano. Geophysical monitoring, including a real- time submarine observatory that continuously monitored Lo¯"ihi’s seismic activity for 3 months, captured some of the volcano’s earthquake swarms. The 1996 swarm, the largest recorded in Hawai"i, was preceded earlier in the year by at least one eruption and accompanied by the formation of a 300-m deep pit crater, Pele’s Pit. Seismic and petrologic data indicate that magma was stored in a 8–9 km deep reservoir prior to the 1996 eruption. -
Explosive Subaqueous Eruptions: the Influence of Volcanic Jets on Eruption Dynamics and Tephra Dispersal in Underwater Eruptions
EXPLOSIVE SUBAQUEOUS ERUPTIONS: THE INFLUENCE OF VOLCANIC JETS ON ERUPTION DYNAMICS AND TEPHRA DISPERSAL IN UNDERWATER ERUPTIONS by RYAN CAIN CAHALAN A DISSERTATION Presented to the Department of Earth ScIences and the Graduate School of the UniversIty of Oregon In partIaL fulfiLLment of the requirements for the degree of Doctor of PhiLosophy December 2020 DISSERTATION APPROVAL PAGE Student: Ryan CaIn CahaLan Title: ExplosIve Subaqueous EruptIons: The Influence of Volcanic Jets on EruptIon DynamIcs and Tephra DIspersaL In Underwater EruptIons This dissertatIon has been accepted and approved in partIaL fulfiLLment of the requirements for the Doctor of PhiLosophy degree in the Department of Earth ScIences by: Dr. Josef Dufek ChaIrperson Dr. Thomas GIachettI Core Member Dr. Paul WaLLace Core Member Dr. KeLLy Sutherland InstItutIonaL RepresentatIve and Kate Mondloch Interim VIce Provost and Dean of the Graduate School OriginaL approvaL sIgnatures are on fiLe wIth the UniversIty of Oregon Graduate School. Degree awarded December 2020 II © 2020 Ryan Cain Cahalan III DISSERTATION ABSTRACT Ryan CaIn CahaLan Doctor of PhiLosophy Department of Earth ScIences December 2020 Title: ExplosIve Subaqueous EruptIons: The Influence of Volcanic Jets on EruptIon DynamIcs and Tephra DIspersaL In Underwater EruptIons Subaqueous eruptIons are often overlooked in hazard consIderatIons though they represent sIgnificant hazards to shipping, coastLInes, and in some cases, aIrcraft. In explosIve subaqueous eruptIons, volcanic jets transport fragmented tephra and exsolved gases from the conduit into the water column. Upon eruptIon the volcanic jet mIxes wIth seawater and rapidly cools. This mIxing and assocIated heat transfer ultImateLy determInes whether steam present in the jet wILL completeLy condense or rise to breach the sea surface and become a subaeriaL hazard. -
Exploring Submarine Arc Volcanoes Steven Carey University of Rhode Island, [email protected]
University of Rhode Island DigitalCommons@URI Graduate School of Oceanography Faculty Graduate School of Oceanography Publications 2007 Exploring Submarine Arc Volcanoes Steven Carey University of Rhode Island, [email protected] Haraldur Sigurdsson University of Rhode Island Follow this and additional works at: https://digitalcommons.uri.edu/gsofacpubs Terms of Use All rights reserved under copyright. Citation/Publisher Attribution Carey, S., and H. Sigurdsson. 2007. Exploring submarine arc volcanoes. Oceanography 20(4):80–89, https://doi.org/10.5670/ oceanog.2007.08. Available at: https://doi.org/10.5670/oceanog.2007.08 This Article is brought to you for free and open access by the Graduate School of Oceanography at DigitalCommons@URI. It has been accepted for inclusion in Graduate School of Oceanography Faculty Publications by an authorized administrator of DigitalCommons@URI. For more information, please contact [email protected]. This article has This been published in or collective redistirbution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The approval portionthe ofwith any permitted articleonly photocopy by is of machine, reposting, this means or collective or other redistirbution SP ec I A L Iss U E On Ocean E X P L O R ATIO N Oceanography , Volume 20, Number 4, a quarterly journal of The 20, Number 4, a quarterly , Volume O ceanography Society. Copyright 2007 by The 2007 by Copyright Society. ceanography Exploring O ceanography Society. All rights All reserved. Society. ceanography O Submarine Arc Volcanoes or Th e [email protected] Send Society. ceanography to: correspondence all B Y S T even C A R E Y an D H A R A LDUR SIGURD ss O N Three quarters of Earth’s volcanic activ- although a significant part of arc volca- tion of tsunamis (Latter, 1981). -
Basaltic Lava Domes, Lava Lakes, and Volcanic Segmentation on the Southern East Pacific Rise Scott M
University of South Carolina Scholar Commons Faculty Publications Earth, Ocean and Environment, School of the 10-10-2000 Basaltic Lava Domes, Lava Lakes, and Volcanic Segmentation on the Southern East Pacific Rise Scott M. White University of South Carolina - Columbia, [email protected] Ken C. Macdonald University of California - Santa Barbara Rachel M. Haymon University of California - Santa Barbara Follow this and additional works at: https://scholarcommons.sc.edu/geol_facpub Part of the Earth Sciences Commons Publication Info Published in Journal of Geophysical Research, Volume 105, Issue B10, 2000, pages 23519-23536. White, S. M., Macdonald, K. C., & Haymon, R. M. (2000). Basaltic lava domes, lava lakes, and volcanic segmentationon the southern East Pacific Rise. Journal of Geophysical Research, 105 (B10), 23519-23536. © Journal of Geophysical Research 2000, American Geophysical Union This Article is brought to you by the Earth, Ocean and Environment, School of the at Scholar Commons. It has been accepted for inclusion in Faculty Publications by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 105,NO. B10, PAGES 23,519-23,536,OCTOBER 10, 2000 Basaltic lava domes, lava lakes, and volcanic segmentation on the southern East Pacific Rise ScottM. White, Ken C. Macdonald,and RachelM. Haymon Departmentof GeologicalSciences and Marine ScienceInstitute, University of California, SantaBarbara Abstract. Meter-scaleDSL-120 sonarmapping and coregisteredArgo -
This Dynamic Earth in January of 1992
View of the planet Earth from the Apollo spacecraft. The Red Sea, which separates Saudi Arabia from the continent of Africa, is clearly visible at the top. (Photograph courtesy of NASA.) Contents Preface Historical perspective Developing the theory Understanding plate motions "Hotspots": Mantle Some unanswered questions Plate tectonics and people Endnotes thermal plumes 1 of 77 2002-01-01 11:52 This pdf-version was edited by Peter Lindeberg in December 2001. Any deviation from the original text is non-intentional. This book was originally published in paper form in February 1996 (design and coordination by Martha Kiger; illustrations and production by Jane Russell). It is for sale for $7 from: U.S. Government Printing Office Superintendent of Documents, Mail Stop SSOP Washington, DC 20402-9328 or it can be ordered directly from the U.S. Geological Survey: Call toll-free 1-888-ASK-USGS Or write to USGS Information Services Box 25286, Building 810 Denver Federal Center Denver, CO 80225 303-202-4700; Fax 303-202-4693 ISBN 0-16-048220-8 Version 1.08 The online edition contains all text from the original book in its entirety. Some figures have been modified to enhance legibility at screen resolutions. Many of the images in this book are available in high resolution from the USGS Media for Science page. USGS Home Page URL: http://pubs.usgs.gov/publications/text/dynamic.html Last updated: 01.29.01 Contact: [email protected] 2 of 77 2002-01-01 11:52 In the early 1960s, the emergence of the theory of plate tectonics started a revolution in the earth sciences. -
The October 1963 Eruption of Kilauea Volcano Hawaii
The October 1963 Eruption of Kilauea Volcano Hawaii GEOLOGICAL SURVEY PROFESSIONAL PAPER 614-C The October 1963 Eruption of Kilauea Volcano Hawaii By JAMES G. MOORE and ROBERT Y. KOYANAGI SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 614-C UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract._______________________________________ Cl Introduction ____________________________________ 1 Distribution of volcanic activity on the east rift zone- 1 Events of 1963 preceding the eruption___--_-_-_--_. 5 Description of the eruption__---_-_-_-_------------ 5 Lava flows_-__---_--____________---_____---____- 7 Earthquakes, tremor, and tilting...-______-___--_-_ 10 Petrology of the lavas. _________________-------_-- 11 References cited _________________________________ 13 ILLUSTRATIONS Page PLATE 1. Geologic map of the central part of the east rift zone of Kilauea Volcano.______________--__-___-_---_--- In pocket FIGURE 1. Map showing the summit region of Kilauea Volcano_________________-__-__.-___._________-_---_--------- C2 2. Diagram showing the longitudinal distribution of eruptive vents on the east rift zone of Kilauea Volcano from 1954 to 1965___________________________________________-_____________--___----_-_-----_--------- :$ 3. Graph showing relations of Kilauean eruptions and collapses, ground tilting, and earthquakes._________---___- "> 4. Graph showing chronology of events during the October 1963 Kilauea east rift eruption.______-___.___._-___- 6 5. Oblique aerial photograph of eruptive vents extending east of Napau Crater_______-_-__---____-_-__-_-_--_- S 6. -
Interpretation of Detections of Volcanic Activity at Ioto Island Obtained From
www.nature.com/scientificreports OPEN Interpretation of detections of volcanic activity at Ioto Island obtained from in situ seismometers and remote hydrophones of the International Monitoring System Hiroyuki Matsumoto1,2*, Mario Zampolli2, Georgios Haralabus2, Jerry Stanley2, James Mattila2 & Nurcan Meral Özel2 In-situ seismic observations identifed that volcanic activity of Ioto (formerly Iwojima), a volcanic island ofshore Japan, increased in early September 2018. Observations of discolored nearshore waters and a splash reported by a local fyover provided evidence for a connection between undersea eruptions and recorded seismic activity. However there remain uncertainties as to when the undersea eruption series commenced and how much of the in-situ seismic activity recorded on the island was associated with volcanic earthquakes versus undersea eruptions. During this period, a large number of underwater acoustic (hydroacoustic) signals were recorded by the Comprehensive Nuclear-Test-Ban Treaty (CTBT) International Monitoring System (IMS) hydroacoustic station HA11, at Wake Island (U.S. Territory), in the northwestern Pacifc Ocean with signals with directions of arrival consistent with sources located at Ioto. The analysis presented here interprets signal features of the remote hydroacoustic recordings provided by HA11 in order to attempt to distinguish between volcanic earthquake signals and undersea eruption signals originating from Ioto. Histograms of hydroacoustic events interpreted as originating from Ioto correlate well with the in-situ seismic observations at Ioto in the early stage of volcanic activity. The results presented suggest that around 75% of the signals detected at HA11 with directions of arrival consistent with Ioto as their origin could be associated with undersea eruptions, supporting the conclusion that the IMS hydroacoustic stations can contribute to volcanic event remote monitoring. -
Hazards from Future Eruptions at Vesuvius (Italy) and Santorini (Greece)
ACCEPTED ON ANNALS OF GEOPHYSICS, 61, 2018; Doi: 10.4401/ag-7761 Explosive volcanoes in the Mediterranean area: hazards from future eruptions at Vesuvius (Italy) and Santorini (Greece) 1 Franco Barberi *, Maria Luisa Carapezza1 1Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma 1, Roma, Italy Explosive volcanoes in the Mediterranean area: hazards from future eruptions at Vesuvius (Italy) and Santorini (Greece) Franco Barberi*, Maria Luisa Carapezza Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma 1, Roma, Italy *Corresponding author email: [email protected] Subject classification: Vesuvius, Santorini, volcanic hazard and risk ABSTRACT Santorini is the site of the famous Minoan eruption of the late Bronze Age and Vesuvius is the type locality for Plinian eruptions. Hazards from the eruption most likely to occur in the near future at these volcanoes are discussed. Downwind zones of Santorini can be affected by minor ash fallout and gas emission from a Vulcanian eruption of Nea Kameni, the most active post-caldera vent. More dangerous would be a sub-Plinian eruption from Columbus, a submarine volcano located 8 km NE of Santorini, whose eruption in 1649-1650 A.D. caused several casualties in Santorini, mostly by wind transported poisoning gas. Vesuvius last erupted in 1944 and its eruptive history includes periods of long quiescence, lasting centuries or tens of centuries, interrupted by violent Plinian or sub-Plinian eruptions. A sub-Plinian eruption is the reference event in the Civil Protection emergency plan. The scenario includes a Red Zone exposed to the risk of being invaded by pyroclastic flows and that should be entirely evacuated before the eruption onset, together with some nearby areas where there is a high risk of roofs collapse by overloading of fallout tephra (nearly 700,000 persons in total). -
Identification of Hydrovolcanism and Its Significance for Hydrocarbon
Xian et al. Journal of Palaeogeography (2018) 7:11 https://doi.org/10.1186/s42501-018-0010-6 Journal of Palaeogeography REVIEW Open Access Identification of hydrovolcanism and its significance for hydrocarbon reservoir assessment: A review Ben-Zhong Xian1,2*, Yan-Xin He1, Hua-Peng Niu1,2, Jun-Hui Wang1,2, Jian-Ping Liu1 and Zhen Wang1 Abstract Investigations of modern volcanic eruptions have demonstrated that ancient volcanic eruptions widely involved water, which was thus named as hydrovolcanic eruptions. Hydrovolcanisms are distinctive in many aspects, such as dynamics, eruptive pattern, texture and structure of rock, and vesicularity. First, normal sediments covered directly by volcanic rocks are the indicators of eruption environments. In addition, microfeatures, special structures, lithofacies or facies associations, and geochemical index of volcanic rocks can also provide significant evidences. Moreover, perlitic texture, quenching fragmentation, surface feature, cementation type, vesicularity, and pillow structure, parallel bedding, large-scale low-angle cross-bedding, antidune cross-bedding of pyroclast are keys to indicating hydrovolcanisms. Clearly, these marks are not equally reliable for identifying eruption environments, and most of them are effective and convincible in limited applications only. For explosive eruptions, the most dependable identification marks include quenching textures, vesicularity in pyroclasts and special large-scale cross-bedding. However, for effusive eruptions, useful indicators mainly include pillow -
Submarine Radial Vents on Mauna Loa Volcano, Hawai`I
Article Geochemistry 3 Volume 7, Number 5 Geophysics 2 May 2006 GeosystemsG Q05001, doi:10.1029/2005GC001086 G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Submarine radial vents on Mauna Loa Volcano, Hawai`i V. Dorsey Wanless and M. O. Garcia Department of Geology and Geophysics, University of Hawai`i, Honolulu, Hawaii 96822, USA ([email protected]) F. A. Trusdell Hawaiian Volcano Observatory, U.S. Geological Survey, Hawai`i National Park, Hawaii 96718, USA J. M. Rhodes Department of Geosciences, University of Massachusetts, Amherst, Massachusetts 01003, USA M. D. Norman Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia Dominique Weis Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, BC, Canada V6T 1Z4 D. J. Fornari and M. D. Kurz Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Herve´ Guillou Laboratorie des Sciences du Climat et de l’Environnement Domaine du CNRS, F-91198 Gif sur Yvette, France [1] A 2002 multibeam sonar survey of Mauna Loa’s western flank revealed ten submarine radial vents and three submarine lava flows. Only one submarine radial vent was known previously. The ages of these vents are constrained by eyewitness accounts, geologic relationships, Mn-Fe coatings, and geochemical stratigraphy; they range from 128 years B.P. to possibly 47 ka. Eight of the radial vents produced degassed lavas despite eruption in water depths sufficient to inhibit sulfur degassing. These vents formed truncated cones and short lava flows. Two vents produced undegassed lavas that created ‘‘irregular’’ cones and longer lava flows. -
Twenty Thousand Leagues Under The
1870 TWENTY THOUSAND LEAGUES UNDER THE SEA Jules Verne Verne, Jules (1828-1905) - French novelist known as “the man who invented the future.” He created a unique blend of science and adventure in his very popu- lar and scientifically prophetic stories. A precursor of modern science fiction, he influenced the work of H.G. Wells, among others. Twenty Thousand Leagues un- der the Sea (1870) - Verne’s remarkable romance about a strange underwater craft piloted by the eccentric Captain Nemo predicted the advent of the deep-sea sub- marine. PART I. CHAPTER I. A SHIFTING REEF. THE year 1866 was signalized by a remarkable incident, a mysterious and in- explicable phenomenon, which doubtless no one has yet forgotten. Not to men- tion rumors which agitated the maritime population, and excited the public mind, even in the interior of continents, seafaring men were particularly excited. Mer- chants, common sailors, captains of vessels, skippers, both of Europe and Amer- ica, naval officers of all countries, and the Governments of several states on the two continents, were deeply interested in the matter. For some time past, vessels had been met by “an enormous thing,” a long ob- ject, spindle-shaped, occasionally phosphorescent, and infinitely larger and more rapid in its movements than a whale. The facts relating to this apparition (entered in various log books) agreed in most respects as to the shape of the object or creature in question, the untiring ra- pidity of its movements, its surprising power of locomotion, and the peculiar life with which it seemed endowed. If it was a cetacean, it surpassed in size all those hitherto classified in science. -
Direct Observation of a Submarine Volcanic Eruption from a Sea-¯Oor
letters to nature 28. Malmgren, B., Kucera, M., Nyberg, J. & Waelbroeck, C. Comparison of available statistical and maximum temperature recorded inside VSM2 during the eruption arti®cial neural network techniques for estimating past sea-surface temperatures from planktonic was only 7.5 8C (Fig. 3)Ðremarkably low, considering that the foraminifera census data. Palaeoceanography (in the press). 29. Bondevik, S., Birks, H. H., Gulliksen, S. & Mangerud, J. Late Weichselian marine 14C reservoir ages at instrument was sitting atop basaltic lava that was probably erupted the western coast of Norway. Quat. Res. 52, 104±114 (1999). at ,1,190 8C (M. Per®t, personal communication). This was 30. Labeyrie, L. et al. Surface and deep hydrology of the northern Atlantic Ocean during the last 150,000 apparently due to the thermal insulation provided by the surface years. Phil. Trans. R. Soc. Lond. 348, 255±264 (1995). crust that forms (and quickly thickens) when submarine lava ¯ows Supplementary information is available on Nature's World-Wide Web site come into contact with frigid sea water13. (http://www.nature.com) or as paper copy from the London editorial of®ce of Nature. The northern end of the 1998 lava ¯ow where VSM2 was located (Fig. 2) is a long, narrow sheet ¯ow4. Submarine sheet ¯ows are Acknowledgements thought to form by brief, relatively high-effusion-rate eruptions8,9. We thank E. Bard and G. Siani for discussions and comments. The data were acquired in Recent models10,11 suggest that such ¯ows initially advance as thin collaboration with T. van Weering, J.-L. Turon, M.